On the trail of fluids in the northernmost intracontinental earthquake swarm areas of the Leipzig-Regensburg fault zone, Germany
The Leipzig-Regensburg fault zone is documented as a band of seismic activity extending northwards from the earthquake swarm region NW-Bohemia/Vogtland at the Czech-German border area and is intersected by several Hercynian fault zones. Along the fault zone, there are several earthquake swarm areas,...
Gespeichert in:
| Veröffentlicht in: | Journal of seismology 2023-08, Vol.27 (4), p.573-597 |
|---|---|
| Hauptverfasser: | , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 597 |
|---|---|
| container_issue | 4 |
| container_start_page | 573 |
| container_title | Journal of seismology |
| container_volume | 27 |
| creator | van Laaten, Marcel Wegler, Ulrich Eulenfeld, Tom |
| description | The Leipzig-Regensburg fault zone is documented as a band of seismic activity extending northwards from the earthquake swarm region NW-Bohemia/Vogtland at the Czech-German border area and is intersected by several Hercynian fault zones. Along the fault zone, there are several earthquake swarm areas, the northernmost of which are Schöneck and Werdau. In this study, we investigate the presumably fluid-induced earthquake swarm activity of the Schöneck and Werdau area. For this purpose, we apply two methods: local earthquake tomography and receiver functions to identify the structural composition of the crust, the areas affected by fluids and the origin of the fluids. We detected potential fluid paths characterised by high Vp/Vs ratios and granite intrusions nearby the swarms characterised by low Vp/Vs anomalies. Receiver function analysis yields the Moho at 25 to 33 km depth and two seismic discontinuities at 55 km and 68 km depth. |
| doi_str_mv | 10.1007/s10950-023-10146-8 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2852189875</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2852189875</sourcerecordid><originalsourceid>FETCH-LOGICAL-c363t-41ed2fb726d66fe9f72760b859eae2442a9d0727ca9e7a2cd7cfecfba2506c333</originalsourceid><addsrcrecordid>eNp9UE1LxDAULKLguvoHPAW8Ws1H2yRHWXQVFhZEwVtI25fatZvuJimye_Knm7WCN0_z3ryZeTBJcknwDcGY33qCZY5TTFlKMMmKVBwlE5LzuOb87TjOTLA0KzJ5mpx5v8IYSyHZJPlaWhTeAQWn2w71BpluaGuP2pG2vYvg7Lr3IXJRVfU2tBZs0B0CHa_bQX8A8p_arZF2oP0h5eBdQLvZt036DA1YXw6uQUYPXUD73sI1moNba7s7T06M7jxc_OI0eX24f5k9povl_Gl2t0grVrCQZgRqakpOi7ooDEjDKS9wKXIJGmiWUS1rHLlKS-CaVjWvDFSm1DTHRcUYmyZXY-7G9dsBfFCrfnA2vlRU5JQIKXgeVXRUVa733oFRG9eutdspgtWhaTU2rWLT6qdpJaKJjSYfxbYB9xf9j-sbUgaEHA</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2852189875</pqid></control><display><type>article</type><title>On the trail of fluids in the northernmost intracontinental earthquake swarm areas of the Leipzig-Regensburg fault zone, Germany</title><source>SpringerLink Journals</source><creator>van Laaten, Marcel ; Wegler, Ulrich ; Eulenfeld, Tom</creator><creatorcontrib>van Laaten, Marcel ; Wegler, Ulrich ; Eulenfeld, Tom</creatorcontrib><description>The Leipzig-Regensburg fault zone is documented as a band of seismic activity extending northwards from the earthquake swarm region NW-Bohemia/Vogtland at the Czech-German border area and is intersected by several Hercynian fault zones. Along the fault zone, there are several earthquake swarm areas, the northernmost of which are Schöneck and Werdau. In this study, we investigate the presumably fluid-induced earthquake swarm activity of the Schöneck and Werdau area. For this purpose, we apply two methods: local earthquake tomography and receiver functions to identify the structural composition of the crust, the areas affected by fluids and the origin of the fluids. We detected potential fluid paths characterised by high Vp/Vs ratios and granite intrusions nearby the swarms characterised by low Vp/Vs anomalies. Receiver function analysis yields the Moho at 25 to 33 km depth and two seismic discontinuities at 55 km and 68 km depth.</description><identifier>ISSN: 1383-4649</identifier><identifier>EISSN: 1573-157X</identifier><identifier>DOI: 10.1007/s10950-023-10146-8</identifier><language>eng</language><publisher>Dordrecht: Springer Netherlands</publisher><subject>Anomalies ; Earth and Environmental Science ; Earth Sciences ; Earthquakes ; Fault lines ; Fault zones ; Fluids ; Function analysis ; Geological faults ; Geophysics/Geodesy ; Geotechnical Engineering & Applied Earth Sciences ; Hydrogeology ; Moho ; Seismic activity ; Seismic discontinuities ; Seismology ; Structural Geology ; Tomography</subject><ispartof>Journal of seismology, 2023-08, Vol.27 (4), p.573-597</ispartof><rights>The Author(s) 2023</rights><rights>The Author(s) 2023. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c363t-41ed2fb726d66fe9f72760b859eae2442a9d0727ca9e7a2cd7cfecfba2506c333</citedby><cites>FETCH-LOGICAL-c363t-41ed2fb726d66fe9f72760b859eae2442a9d0727ca9e7a2cd7cfecfba2506c333</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10950-023-10146-8$$EPDF$$P50$$Gspringer$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10950-023-10146-8$$EHTML$$P50$$Gspringer$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>van Laaten, Marcel</creatorcontrib><creatorcontrib>Wegler, Ulrich</creatorcontrib><creatorcontrib>Eulenfeld, Tom</creatorcontrib><title>On the trail of fluids in the northernmost intracontinental earthquake swarm areas of the Leipzig-Regensburg fault zone, Germany</title><title>Journal of seismology</title><addtitle>J Seismol</addtitle><description>The Leipzig-Regensburg fault zone is documented as a band of seismic activity extending northwards from the earthquake swarm region NW-Bohemia/Vogtland at the Czech-German border area and is intersected by several Hercynian fault zones. Along the fault zone, there are several earthquake swarm areas, the northernmost of which are Schöneck and Werdau. In this study, we investigate the presumably fluid-induced earthquake swarm activity of the Schöneck and Werdau area. For this purpose, we apply two methods: local earthquake tomography and receiver functions to identify the structural composition of the crust, the areas affected by fluids and the origin of the fluids. We detected potential fluid paths characterised by high Vp/Vs ratios and granite intrusions nearby the swarms characterised by low Vp/Vs anomalies. Receiver function analysis yields the Moho at 25 to 33 km depth and two seismic discontinuities at 55 km and 68 km depth.</description><subject>Anomalies</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earthquakes</subject><subject>Fault lines</subject><subject>Fault zones</subject><subject>Fluids</subject><subject>Function analysis</subject><subject>Geological faults</subject><subject>Geophysics/Geodesy</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Hydrogeology</subject><subject>Moho</subject><subject>Seismic activity</subject><subject>Seismic discontinuities</subject><subject>Seismology</subject><subject>Structural Geology</subject><subject>Tomography</subject><issn>1383-4649</issn><issn>1573-157X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9UE1LxDAULKLguvoHPAW8Ws1H2yRHWXQVFhZEwVtI25fatZvuJimye_Knm7WCN0_z3ryZeTBJcknwDcGY33qCZY5TTFlKMMmKVBwlE5LzuOb87TjOTLA0KzJ5mpx5v8IYSyHZJPlaWhTeAQWn2w71BpluaGuP2pG2vYvg7Lr3IXJRVfU2tBZs0B0CHa_bQX8A8p_arZF2oP0h5eBdQLvZt036DA1YXw6uQUYPXUD73sI1moNba7s7T06M7jxc_OI0eX24f5k9povl_Gl2t0grVrCQZgRqakpOi7ooDEjDKS9wKXIJGmiWUS1rHLlKS-CaVjWvDFSm1DTHRcUYmyZXY-7G9dsBfFCrfnA2vlRU5JQIKXgeVXRUVa733oFRG9eutdspgtWhaTU2rWLT6qdpJaKJjSYfxbYB9xf9j-sbUgaEHA</recordid><startdate>20230801</startdate><enddate>20230801</enddate><creator>van Laaten, Marcel</creator><creator>Wegler, Ulrich</creator><creator>Eulenfeld, Tom</creator><general>Springer Netherlands</general><general>Springer Nature B.V</general><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope></search><sort><creationdate>20230801</creationdate><title>On the trail of fluids in the northernmost intracontinental earthquake swarm areas of the Leipzig-Regensburg fault zone, Germany</title><author>van Laaten, Marcel ; Wegler, Ulrich ; Eulenfeld, Tom</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c363t-41ed2fb726d66fe9f72760b859eae2442a9d0727ca9e7a2cd7cfecfba2506c333</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Anomalies</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Earthquakes</topic><topic>Fault lines</topic><topic>Fault zones</topic><topic>Fluids</topic><topic>Function analysis</topic><topic>Geological faults</topic><topic>Geophysics/Geodesy</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Hydrogeology</topic><topic>Moho</topic><topic>Seismic activity</topic><topic>Seismic discontinuities</topic><topic>Seismology</topic><topic>Structural Geology</topic><topic>Tomography</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>van Laaten, Marcel</creatorcontrib><creatorcontrib>Wegler, Ulrich</creatorcontrib><creatorcontrib>Eulenfeld, Tom</creatorcontrib><collection>Springer Nature OA Free Journals</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Journal of seismology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>van Laaten, Marcel</au><au>Wegler, Ulrich</au><au>Eulenfeld, Tom</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>On the trail of fluids in the northernmost intracontinental earthquake swarm areas of the Leipzig-Regensburg fault zone, Germany</atitle><jtitle>Journal of seismology</jtitle><stitle>J Seismol</stitle><date>2023-08-01</date><risdate>2023</risdate><volume>27</volume><issue>4</issue><spage>573</spage><epage>597</epage><pages>573-597</pages><issn>1383-4649</issn><eissn>1573-157X</eissn><abstract>The Leipzig-Regensburg fault zone is documented as a band of seismic activity extending northwards from the earthquake swarm region NW-Bohemia/Vogtland at the Czech-German border area and is intersected by several Hercynian fault zones. Along the fault zone, there are several earthquake swarm areas, the northernmost of which are Schöneck and Werdau. In this study, we investigate the presumably fluid-induced earthquake swarm activity of the Schöneck and Werdau area. For this purpose, we apply two methods: local earthquake tomography and receiver functions to identify the structural composition of the crust, the areas affected by fluids and the origin of the fluids. We detected potential fluid paths characterised by high Vp/Vs ratios and granite intrusions nearby the swarms characterised by low Vp/Vs anomalies. Receiver function analysis yields the Moho at 25 to 33 km depth and two seismic discontinuities at 55 km and 68 km depth.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s10950-023-10146-8</doi><tpages>25</tpages><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1383-4649 |
| ispartof | Journal of seismology, 2023-08, Vol.27 (4), p.573-597 |
| issn | 1383-4649 1573-157X |
| language | eng |
| recordid | cdi_proquest_journals_2852189875 |
| source | SpringerLink Journals |
| subjects | Anomalies Earth and Environmental Science Earth Sciences Earthquakes Fault lines Fault zones Fluids Function analysis Geological faults Geophysics/Geodesy Geotechnical Engineering & Applied Earth Sciences Hydrogeology Moho Seismic activity Seismic discontinuities Seismology Structural Geology Tomography |
| title | On the trail of fluids in the northernmost intracontinental earthquake swarm areas of the Leipzig-Regensburg fault zone, Germany |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-05T01%3A32%3A08IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=On%20the%20trail%20of%20fluids%20in%20the%20northernmost%20intracontinental%20earthquake%20swarm%20areas%20of%20the%20Leipzig-Regensburg%20fault%20zone,%20Germany&rft.jtitle=Journal%20of%20seismology&rft.au=van%20Laaten,%20Marcel&rft.date=2023-08-01&rft.volume=27&rft.issue=4&rft.spage=573&rft.epage=597&rft.pages=573-597&rft.issn=1383-4649&rft.eissn=1573-157X&rft_id=info:doi/10.1007/s10950-023-10146-8&rft_dat=%3Cproquest_cross%3E2852189875%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2852189875&rft_id=info:pmid/&rfr_iscdi=true |